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    <title><![CDATA[1A Collections]]></title>
    <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/browse?tags=lamination&amp;output=rss2</link>
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    <pubDate>Tue, 09 Apr 2024 21:16:18 +0100</pubDate>
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    <item>
      <title><![CDATA[L341
Mudstone, calcareous]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/28</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>L341<br /></strong></h2>
<h2>Mudstone, calcareous</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><h3>Age</h3>
<div class="element-text">
<p>Lower Carboniferous</p>
<h3>Location</h3>
<div class="element-text">
<p>Millstone Grit Series<br />Bowland, West Yorkshire</p>
</div>
</div></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<h3>Hand Specimen</h3>
<div class="element-text">
<p>Very dark grey to black mudstone.<span> </span><br />Faint, fine-scale laminations visible on cut surface.<span> </span><br />Not<span> </span><a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/196">fissile</a><span> </span>- does not readily split along bedding planes.<br />Contains fossils and fossil imprints.<span> </span><br />Some glinting flakes of mica.<span> </span><br />This rock fizzes gently with acid, indicating that it contains some carbonate.<span> </span><br />Weathered to light brown-grey in places.</p>
</div>
</div>
<div class="element">
<h3>Thin-section</h3>
<div class="element-text">Laminations are very clear when the thin-section is held up to the light. They are mainly planar, but some wrap around lighter regions in the rock.<br /><br />Under the microscope, the rock is brown, with fine dark brown streaks, laminated.<br />Mainly carbonate, some white mica, rare quartz.<br />Bioclasts, mainly along bedding surfaces, probably gastropods and bivalves. Some of the shells have been dissolved. The spaces left have been filled by secondary calcite.<br />Sparry carbonate cement.</div>
</div>
<div class="element">
<h3>Rock History</h3>
<div class="element-text">
<p>Fine-grained, so formed in a very low energy environment.<span> </span><br />Shells are too large to have been swept in by such low energy currents, so the shells are in life position.<span> </span><br />If the shells are indeed gastropods and bivalves the rock could be marine or non-marine. The presence of brachiopods<span> </span><em>would</em><span> </span>indicate a marine environment.</p>
</div>
</div>
<div class="element"></div>
<div class="element"></div>
<div class="element">
<h3>Rock Name</h3>
<div class="element-text">calcareous mudstone</div>
</div></div>
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<div class="item-file image-jpeg"><a class="download-file" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/2104f9a268fa0c07974391c7e5b42537.jpg"><img class="thumb" src="https://wserv3.esc.cam.ac.uk/p1acollections/files/square_thumbnails/2104f9a268fa0c07974391c7e5b42537.jpg" alt="L341_HS.jpg" title="L341_HS.jpg"></a></div><div class="item-file image-jpeg"><a class="download-file" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/0d1b0055e9ce25409830de31afcc15e7.jpg"><img class="thumb" src="https://wserv3.esc.cam.ac.uk/p1acollections/files/square_thumbnails/0d1b0055e9ce25409830de31afcc15e7.jpg" alt="L341_TS_ppl.jpg" title="L341_TS_ppl.jpg"></a></div><div class="item-file image-jpeg"><a class="download-file" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/f6f992805d2607a8fd41a0fc8b12aa41.jpg"><img class="thumb" src="https://wserv3.esc.cam.ac.uk/p1acollections/files/square_thumbnails/f6f992805d2607a8fd41a0fc8b12aa41.jpg" alt="L341_TS_xpl.jpg" title="L341_TS_xpl.jpg"></a></div><div class="item-file image-jpeg"><a class="download-file" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/40665952add448e60dd592fd440b8865.jpg"><img class="thumb" src="https://wserv3.esc.cam.ac.uk/p1acollections/files/square_thumbnails/40665952add448e60dd592fd440b8865.jpg" alt="L341b_TS_ppl.jpg" title="L341b_TS_ppl.jpg"></a></div><div class="item-file image-jpeg"><a class="download-file" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/5d38ba3667c7dc71e02797f7fd019b47.jpg"><img class="thumb" src="https://wserv3.esc.cam.ac.uk/p1acollections/files/square_thumbnails/5d38ba3667c7dc71e02797f7fd019b47.jpg" alt="L341b_TS_xpl.jpg" title="L341b_TS_xpl.jpg"></a></div>]]></description>
      <pubDate>Mon, 17 Jun 2019 10:52:33 +0100</pubDate>
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    <item>
      <title><![CDATA[L326
Sandstone, ferruginous arenite]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/25</link>
      <description><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>L326<br /></strong></h2>
<h2>Sandstone, ferruginous arenite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><h3>Specimen Age</h3>
<div class="element-text">Permian<br /><h3>Location</h3>
<div class="element-text">Penrith Sandstone<br />Appleby, Westmorland</div>
</div></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<div class="element">
<h3>Hand Specimen</h3>
<div class="element-text">Reddish brown rock. Medium sand grade.<br />Round to sub-round grains of quartz, often with a thin rim of red hematite. Mainly reddish and pink-brown grains, fewer white grains and very few black grains. Well sorted and well cemented.<br />No fizzing with acid, so does not contain significant carbonate.<span> </span><br /><br />Laminations can be observed in sample L326b. There is an inter-layering of coarser and finer laminae.</div>
</div>
<div class="element">
<h3>Thin-section</h3>
<div class="element-text">
<p>Fine laminations can be seen when the thin-section is held up to the light.<span> </span><br />Moderately well rounded quartz grains with thin rims of hematite, and overgrowths of quartz in optical continuity with the original grain.<span> </span><br />Occasional grains of very fine quartzite, microcline, plagioclase, mica and decomposed fine-grained igneous rocks.<span> </span><br />Siliceous cement and the secondary quartz<span> </span><a href="/p1acollections/items/show/232">overgrowths</a><span> </span>hold this rock together.</p>
<p>The grains are finer as a whole in L326b, and less well rounded.</p>
</div>
</div>
<div class="element">
<h3>Rock History</h3>
<div class="element-text">
<p>Probably deposited in an<span> </span><a href="/p1acollections/items/show/167">aeolian</a><span> </span>environment, since it almost entirely comprises well sorted and well rounded quartz grains.</p>
</div>
</div>
<div class="element"></div>
<div class="element"></div>
<div class="element">
<h3>Rock Name</h3>
<div class="element-text">ferruginous sandstone<br />ferruginous arenite</div>
</div>
</div></div>
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      <pubDate>Mon, 17 Jun 2019 10:28:37 +0100</pubDate>
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